Van Niel, Thomas G.McVicar, Tim RRoderick, Michaelvan Dijk, AlbertRenzullo, Luigi Jvan Gorsel, Eva2015-12-100022-1694http://hdl.handle.net/1885/50523Practical methods to scale 'instantaneous' latent heat flux (λE) estimates from thermal remote sensing to values for daily or longer periods normally rely on the assumption that the evaporative fraction (EF) - the ratio of λE over available energy - remKeywords: Available energy; Correction method; Evaporative fraction; Median errors; Practical method; Self-preservation; Temperate forests; Temporal scaling; Time of day; Energy balance; Interfacial energy; Latent heat; Remote sensing; Surface chemistry; Towers; Wa Evaporation; Evaporative fraction; Evapotranspiration; Integration; Latent heat flux; Self-preservation201110.1016/j.jhydrol.2011.08.0112016-02-24